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海洋补贴在沙漠岛屿上产生了仙人掌林。

Marine subsidies produce cactus forests on desert islands.

机构信息

Next Generation Sonoran Desert Researchers (N-Gen), Tucson, USA.

College of Education, University of Arizona, 1430 E 2nd St, Tucson, AZ, 85721, USA.

出版信息

Sci Rep. 2022 Oct 12;12(1):17110. doi: 10.1038/s41598-022-21133-3.

Abstract

In island systems, nitrogen-rich seabird guano is a marine subsidy that can shape terrestrial plant communities. In zones of nutrient upwelling such as the Gulf of California, copious seabird guano is commonplace on bird islands. Several bird islands host regionally unique cactus forests, especially of the large columnar cactus, cardón (Pachycereus pringlei). We show that a chain of interactions across the land-sea interface yields an allochthonous input of nitrogen in the form of seabird guano, fueling the production of some of the densest cactus populations in the world. Fish, seabird, guano, soil, and cactus samples were taken from the representative seabird island of San Pedro Mártir for nitrogen stable isotope ratio measurements, which were compared to soil and cactus samples from other seabird and non-seabird Gulf islands and terrestrial ecosystems throughout the range of the cardón. Isla San Pedro Mártir δN values are distinctively high, ranging from fish + 17.7, seabird + 19.7, guano + 14.8, soil + 34.3 and cactus + 30.3 compared to average values across non-bird sites of + 13.0 (N = 213, S.D. = 3.7) for soil and + 9.8 (N = 212, S.D. = 3.4) for cactus. These δN values are among the highest ever reported for plants. Seabird island soil and cactus δN values were consistently significantly enriched relative to mainland and non-bird islands, a relationship expected due to the progressive volatilization of N rich ammonia from decomposing guano deposits. Our findings demonstrate that seabird-mediated marine nutrient deposits provide the source for solubilized nitrogen on desert islands, which stimulate terrestrial plant production in the cardón cactus beyond that seen in either mainland ecosystems or non-seabird islands.

摘要

在岛屿系统中,富含氮的海鸟粪便是一种海洋补贴,可以塑造陆地植物群落。在加利福尼亚湾等营养上升区,丰富的海鸟粪便是鸟类岛屿的常见现象。几个鸟类岛屿拥有地区独特的仙人掌森林,特别是大型柱状仙人掌,如龙舌兰(Pachycereus pringlei)。我们表明,陆海界面的一系列相互作用产生了以海鸟粪形式的外源氮输入,为世界上一些最密集的仙人掌种群的产生提供了燃料。从圣佩德罗·马蒂尔(San Pedro Mártir)代表性海鸟岛采集了鱼类、海鸟、鸟粪、土壤和仙人掌样本,用于进行氮稳定同位素比测量,并与来自其他海鸟和非海鸟海湾岛屿以及龙舌兰分布范围内的陆地生态系统的土壤和仙人掌样本进行了比较。圣佩德罗·马蒂尔岛的 δN 值明显较高,范围从鱼类+17.7、海鸟+19.7、鸟粪+14.8、土壤+34.3 和仙人掌+30.3,而跨非鸟类地点的平均值为+13.0(N=213,S.D.=3.7),土壤为+9.8(N=212,S.D.=3.4),仙人掌为。这些 δN 值是植物中报告的最高值之一。海鸟岛土壤和仙人掌的 δN 值与大陆和非鸟类岛屿相比始终明显富集,这种关系是由于分解的鸟粪沉积物中富含氮的氨的逐渐挥发所致。我们的研究结果表明,海鸟介导的海洋养分沉积为沙漠岛屿上的可溶性氮提供了来源,这刺激了龙舌兰仙人掌在陆地植物中的产生,其程度超过了大陆生态系统或非海鸟岛屿的产生。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2460/9556768/1c278b1fa664/41598_2022_21133_Fig1_HTML.jpg

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